By David B. Stone (auth.), Alan E. M. Nairn, Francis G. Stehli, Seiya Uyeda (eds.)
ISBN-10: 1461580412
ISBN-13: 9781461580416
ISBN-10: 1461580439
ISBN-13: 9781461580430
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Additional info for The Ocean Basins and Margins: Volume 7B: The Pacific Ocean
Example text
Lag 19. a wllb ero .. 15-2 (rrom Scholl. Vamor and $I01llnSOn 1983) ALEUTIAN AIDGE, TAENCH AND AOJACENT BASINS 172-e Bering Sea-Aleutian Are, Alaska 37 Another physiographie observation of interest is that west of Seguam Volcano (Fig. 16), the volcanoes of the present aetive are are all perehed on the northernmost edge of the ridge. The exeeption to this oeeurs where the situation is eonfused by the junetion of Bowers Ridge with the Aleutian Are. In addition to physiographie studies, sources of information used to deduee the geologieal history of the Aleutian Are and its relationship to the Bering Sea, inc1ude seismieity studies aided by investigations related to nuc1ear tests on Amehitka Island (Engdahl, 1971, 1972; Jaeob, 1972), marine geophysieal investigations, dredge hauls, and aseries of Oeep Sea Orilling Projeet (OSOP) holes.
The surface of the acoustic basement of the Black Hills Ridge is unconformably overlain by the sediments of the main layered sequence. The erosional unconformity appears to represent a wave-cut surface which, ifreal, indicates subsidence on the order of 2 km on the southwest side of the St. George Basin. Miocene a older Fig. 14. Generalized cross section across the Bering Sea margin. (From Marlow et al. ) -:,-;?? --~ V. E. ) ALEUTIAN BASIN sr GEORGE BASIN ----I . - --~ -" '-~~~ ~ ~~ :3 ---=~18 5 ~ ~~ DIatom ooze; and " ' .
Lawrence subbasin north and east of St. Lawrence Island and the Stuart subbasin north and east of the Yukon Delta. These two areas are divided by the Yukon Horst. Figure 8 shows the generalized structure as redrawn from Fisher et al. (1982). Both parts of the basin show considerably deeper basement depths than were initially estimated by Scholl and Hopkins (1969). The deepest parts of the St. 5 km. Farther west than the St. Lawrence subbasin, the basement depths are subdued, seldom exceeding 2 km.
The Ocean Basins and Margins: Volume 7B: The Pacific Ocean by David B. Stone (auth.), Alan E. M. Nairn, Francis G. Stehli, Seiya Uyeda (eds.)
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